Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China
Abstract We investigated the relationship between convective activity and F‐region short‐period ionospheric disturbances at middle latitudes from 2018 to 2020. The ionospheric variations were extracted from the total electron content (TEC) data obtained by the BeiDou geostationary orbit receiver in...
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Wiley
2022-10-01
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Online Access: | https://doi.org/10.1029/2022SW003140 |
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author | Zhenlin Yang Sheng‐Yang Gu Yusong Qin Chen‐Ke‐Min Teng Fuqing Huang Wenjie Sun Xiankang Dou |
author_facet | Zhenlin Yang Sheng‐Yang Gu Yusong Qin Chen‐Ke‐Min Teng Fuqing Huang Wenjie Sun Xiankang Dou |
author_sort | Zhenlin Yang |
collection | DOAJ |
description | Abstract We investigated the relationship between convective activity and F‐region short‐period ionospheric disturbances at middle latitudes from 2018 to 2020. The ionospheric variations were extracted from the total electron content (TEC) data obtained by the BeiDou geostationary orbit receiver in Wuhan, China, while the convective activities were represented by precipitation data from the fifth generation European Center for Medium‐Range Weather Forecasts Reanalysis (ERA5). Additionally, an ionosonde located in Wuhan, China, was used to study the variation in the sporadic E (Es)‐layer. Seasonal variations in the convective activity and TEC disturbances were studied. It was found that short‐period ionospheric disturbances occurred mainly around summer midnight and around the June solstice. In addition, the correlations between convective activity and the ionosphere have also been studied. A positive correlation between precipitation and short‐period ionospheric disturbances was found. Similarly, precipitation and foEs also had a positive correlation. By analyzing the precipitation azimuth and upward propagation of convective gravity waves, we proposed a possible coupling mechanism between the ionosphere and the troposphere, through which convective gravity waves could indirectly affect F‐region short‐period ionospheric disturbances by modulating the Es‐layer. |
format | Article |
id | doaj-art-7d98f9e23bea41c1b145581c55080829 |
institution | Kabale University |
issn | 1542-7390 |
language | English |
publishDate | 2022-10-01 |
publisher | Wiley |
record_format | Article |
series | Space Weather |
spelling | doaj-art-7d98f9e23bea41c1b145581c550808292025-01-14T16:30:48ZengWileySpace Weather1542-73902022-10-012010n/an/a10.1029/2022SW003140Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, ChinaZhenlin Yang0Sheng‐Yang Gu1Yusong Qin2Chen‐Ke‐Min Teng3Fuqing Huang4Wenjie Sun5Xiankang Dou6Electronic Information School Wuhan University Wuhan ChinaElectronic Information School Wuhan University Wuhan ChinaElectronic Information School Wuhan University Wuhan ChinaBeijing Institute of Applied Meteorology Beijing ChinaSchool of Earth and Space Sciences CAS Key Laboratory of Geospace Environment University of Science and Technology of China Hefei ChinaBeijing National Observatory of Space Environment Institute of Geology and Geophysics Chinese Academy of Sciences Beijing ChinaElectronic Information School Wuhan University Wuhan ChinaAbstract We investigated the relationship between convective activity and F‐region short‐period ionospheric disturbances at middle latitudes from 2018 to 2020. The ionospheric variations were extracted from the total electron content (TEC) data obtained by the BeiDou geostationary orbit receiver in Wuhan, China, while the convective activities were represented by precipitation data from the fifth generation European Center for Medium‐Range Weather Forecasts Reanalysis (ERA5). Additionally, an ionosonde located in Wuhan, China, was used to study the variation in the sporadic E (Es)‐layer. Seasonal variations in the convective activity and TEC disturbances were studied. It was found that short‐period ionospheric disturbances occurred mainly around summer midnight and around the June solstice. In addition, the correlations between convective activity and the ionosphere have also been studied. A positive correlation between precipitation and short‐period ionospheric disturbances was found. Similarly, precipitation and foEs also had a positive correlation. By analyzing the precipitation azimuth and upward propagation of convective gravity waves, we proposed a possible coupling mechanism between the ionosphere and the troposphere, through which convective gravity waves could indirectly affect F‐region short‐period ionospheric disturbances by modulating the Es‐layer.https://doi.org/10.1029/2022SW003140ionospheric disturbancesconvectionBeiDou GEOgravity wavessporadic E layersTEC |
spellingShingle | Zhenlin Yang Sheng‐Yang Gu Yusong Qin Chen‐Ke‐Min Teng Fuqing Huang Wenjie Sun Xiankang Dou Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China Space Weather ionospheric disturbances convection BeiDou GEO gravity waves sporadic E layers TEC |
title | Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China |
title_full | Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China |
title_fullStr | Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China |
title_full_unstemmed | Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China |
title_short | Statistical Study of F‐Region Short Period Ionospheric Disturbances Related to Convection in the Lower Atmosphere Over Wuhan, China |
title_sort | statistical study of f region short period ionospheric disturbances related to convection in the lower atmosphere over wuhan china |
topic | ionospheric disturbances convection BeiDou GEO gravity waves sporadic E layers TEC |
url | https://doi.org/10.1029/2022SW003140 |
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